Scientists found Alternating bands of magnetism.
No, they are silly.
Bands of rock on the seafloor showing alternating magnetic orientation indicate times when the Earth's magnetic field has reversed. These bands are created as new oceanic crust forms at mid-ocean ridges and records the direction of the Earth's magnetic field at the time of its formation. Studying these bands provides insight into the history of Earth's magnetic field reversals.
Earth's alternating magnetic bands are called magnetic reversals or geomagnetic reversals. These reversals are periods in Earth's history where the magnetic field flips, with the north and south magnetic poles reversing positions. They can be detected in the rock record and provide valuable information about Earth's geological history.
Magnetic bands for balance
reversed itself in the past. hth :)
The magnetic bands in the eastern Pacific Ocean are more spread out because the spreading rate of the seafloor there is slower compared to the Mid Atlantic Ridge. Slower spreading rates lead to wider magnetic bands as less new crust is being formed over a longer period of time. Conversely, faster spreading rates at the Mid Atlantic Ridge result in narrower magnetic bands due to the more rapid formation of new crust.
Van Allen Belt
No, rubber bands are typically made of non-magnetic materials like rubber or latex, so they do not stick to magnets. Magnets attract materials with iron, nickel, or cobalt in them, but rubber bands do not contain these magnetic materials.
True. Bands of magnetic material in the sea floor that have opposite poles or exhibit magnetic reversal provide evidence for sea floor spreading. This is because as new oceanic crust forms at mid-ocean ridges, Earth's magnetic field periodically reverses, creating magnetic stripes on the ocean floor that align with the direction of the magnetic field at that time.
true
The number of pigment bands seen in a chromatography experiment will depend on the number of different pigments present in the sample being analyzed. Each pigment will typically appear as a distinct band on the chromatogram.
If true, it would indicate that the divergent plates of the eastern Pacific are spreading at a faster rate than the plates of the Mid-Atlantic Ridge.